The role of strain hardening in the transition from dislocation-mediated to frictional deformation of marbles within the Karakoram Fault Zone, NW India

David Wallis, Geoffrey E. Lloyd, Lars N. Hansen

Research output: Contribution to journalArticlepeer-review

3 Scopus citations

Abstract

The onset of frictional failure and potentially seismogenic deformation in carbonate rocks undergoing exhumation within fault zones depends on hardening processes that reduce the efficiency of aseismic dislocation-mediated deformation as temperature decreases. However, few techniques are available for quantitative analysis of dislocation slip system activity and hardening in natural tectonites. Electron backscatter diffraction maps of crystal orientations offer one such approach via determination of Schmid factors, if the palaeostress conditions can be inferred and the critical resolved shear stresses of slip systems are constrained. We analyse calcite marbles deformed in simple shear within the Karakoram Fault Zone, NW India, to quantify changes in slip system activity as the rocks cooled during exhumation. Microstructural evidence demonstrates that between ∼300 °C and 200–250 °C the dominant deformation mechanisms transitioned from dislocation-mediated flow to twinning and frictional failure. However, Schmid factor analysis, considering critical resolved shear stresses for yield of undeformed single crystals, indicates that the fraction of grains with sufficient resolved shear stress for glide apparently increased with decreasing temperature. Misorientation analysis and previous experimental data indicate that strain-dependent work hardening is responsible for this apparent inconsistency and promoted the transition from dislocation-mediated flow to frictional, and potentially seismogenic, deformation.

Original languageEnglish (US)
Pages (from-to)25-37
Number of pages13
JournalJournal of Structural Geology
Volume107
DOIs
StatePublished - Feb 2018
Externally publishedYes

Bibliographical note

Funding Information:
We thank Richard Phillips and Ernie Rutter for providing the sample for this study, Cees Passchier for his editorial handling of the manuscript, and Hans de Bresser and Elisabetta Mariani for their reviews. We are grateful to Rick Law, Gordon Lister and Andrew Turner for helpful discussions. David Wallis and Lars Hansen acknowledge support from the Natural Environment Research Council grant NE/M000966/1 . Data reported in this study are available on request from the corresponding author.

Publisher Copyright:
© 2017 Elsevier Ltd

Keywords

  • Calcite
  • Karakoram Fault Zone
  • Resolved shear stress
  • Schmid factor
  • Seismogenesis
  • Strain hardening

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